Search results for " ROC"

showing 10 items of 951 documents

L'innovazione di Rocco Chinnici

2004

Il saggio si sofferma sulle innovazioni introdotte dal magistrato Rocco Chinnici nelle indagini su Cosa nostra

Settore SPS/12 - Sociologia Giuridica Della Devianza E Mutamento Socialeindagini finanziarie Rocco Chinnici mafie
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Contrasting metamorphic evolution of metasedimentary rocks from the Çine and Selimiye nappes in the Anatolide belt, western Turkey

2003

P-T conditions, mineral isograds, the relation of the latter to foliation planes and kinematic indicators are used to elucidate the tectonic nature and evolution of a shear zone in an orogen exhumed from mid- crustal depths in western Turkey. Furthermore, we discuss whether simple monometamorphic fabrics of rock units from different nappes result from one single orogeny or are related to different orogenies. Metasedimentary rocks from the Cine and Selimiye nappes at the southern rim of the Anatolide belt of western Turkey record different metamorphic evolutions. The Eocene Selimiye shear zone separates both nappes. Metasedimentary rocks from the Cine nappe underneath the Selimiye shear zone…

Shear (geology)Geochemistry and PetrologyGreenschistMetamorphic rockGeochemistryMetamorphismGeologyOrogenyShear zoneMetamorphic faciesGeologyNappeJournal of Metamorphic Geology
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1999

Two retrograde, amphibolite facies shear zones were studied to explore the relationship between retrograde mineral reactions, volume strain, fluid flow, mylonitization, and coaxial versus noncoaxial deformation. The two shear zones are the contractional Mafwewu Hills shear zone and the transcurrently displacing Mkamasa River shear zone of northern Malawi. In general, shear-zone formation is characterized by the breakdown of feldspar and biotite and the formation of sillimanite, quartz, and water. Silica, alkali, and alkali earth elements were mobile. Mass-balance calculations, based on major- and trace-element geochemistry, indicate as much as 50%–60% volume loss in mylonite. Fluid to rock …

Shearing (physics)LineationShear (geology)MineralogyGeologyShear zoneSillimanitePetrologyMetamorphic faciesGeologyMyloniteWall rockGeological Society of America Bulletin
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Sequence stratigraphy of a mesozoic carbonate platform-to-basin system in Western sicily

2009

Abstract Sequence stratigraphic studies of the Triassic through Paleogene carbonate successions of platform, slope and basin in western Sicily (Palermo and Termini Imerese Mountains) have identified a sedimentary cyclicity mostly caused by relative oscillations of sea level. The stratigraphic successions of the Imerese and Panormide palaeogeographic domains of the southern Tethyan continental margin were studied with physical-stratigraphy and facies analysis to reconstruct the sedimentary evolution of this platform-to-basin system. The Imerese Basin is characterized by a carbonate and siliceous-calcareous succession, 1200–1400m thick, Late Triassic to Eocene in age. The strata display a typ…

Shelf-to-basin system sedimentologyQE1-996.5tectono-eustatic cyclesSettore GEO/02 - Geologia Stratigrafica E SedimentologicaCarbonate platformTransgressive/regressive cyclesGeologyEnvironmental Science (miscellaneous)Paleontologychemistry.chemical_compoundchemistryContinental marginFaciesTectono-eustatic cycleGeneral Earth and Planetary SciencesCarbonateSedimentary rockSequence stratigraphyProgradationMesozoic western SicilyPaleogeneGeology
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The Geologic History of the Marginal Basins Along the North Shore of the Gulf of Guinea

1973

The North shore of the Gulf of Guinea forms the coastline of Liberia, the Ivory Coast, Ghana, Togo, Dahomey, Nigeria, and the Cameroons (Fig. 1). The westernmost point of the coastal region to be discussed here is Cape Palmas (long 8° W) on the border between Liberia and the Ivory Coast. The easternmost limit is formed by the Cameroons Bight at long 9° 30′ E. The marginal basins are limited to the north by the upper Guinea arch which stretches for more than 2000 km in a west-east direction from Liberia to the Cameroons. In this arch region the metamorphic basement is exposed over wide areas. Some of the details of this basement are discussed by Hurley and Rand, and by Grant in this book. Fo…

ShorePrecambriangeographygeography.geographical_feature_categoryBasement (geology)OceanographyContinental marginShieldCapeMetamorphic rockGeologic historyArchaeologyGeology
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Prefazione

2013

Sicilia Rocca di Cefalù
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Il contributo degli architetti siciliani ai concorsi per le nuove chiese italiane della CEI

2015

Il saggio analizza il contributo degli architetti siciliani ai concorsi per le nuove chiese italiane della CEI. Nell’ambito di tale lunga esperienza promossa dalla CEI, il contributo degli architetti siciliani alla realizzazione delle nuove chiese italiane appare particolarmente significativo e si distingue per una costante presenza in tutti i concorsi e per la qualità dei risultati raggiunti attraverso l’esplorazione di temi progettuali tutti interni al processo di rinnovamento liturgico e rituale. Pasquale Culotta e Giuseppe (Bibi) Leone sono i primi a esordire nell’iniziale concorso indetto nel 1998 con il progetto per la parrocchia di San Giovan Battista in Lecce. L’anno successivo, Vin…

Sicilian architects Italian Episcopal Conference new Italian churches Pasquale Culotta Bibi Leone Vincenzo Melluso Marcello Panzarella Andrea Sciascia competitionSettore ICAR/14 - Composizione Architettonica E Urbananuove chiese italiane Conferenza Episcopale Italiana CEI architetti siciliano rinnovamento liturgico Pasquale Culotta Giuseppe Leone Vincenzo Melluso Marcello Panzarella Andrea Sciascia Sebastiano Triscari Vito Corte parrocchia di San Giovan Battista in Lecce complesso parrocchiale di Gesù Maestro in Potenza parrocchia di Santa Maria Roccella in località Roccelletta a Catanzaro chiesa parrocchiale di Santa Maria del Carmine ad Avellino complesso parrocchiale di San Giorgio Martire in Dresdano parrocchia di San Giacomo Apostolo in Ferrara
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Census of the Sicilian rock partridge Alectoris graeca whitakeri population in ZPS ITA010029 Monte Cofano, Capo San Vito and Monte Sparagio

2013

During the project "LIFE09 NAT/IT/000099-SICALECONS-Urgent actions for the conservation of Alectoris graeca whitakeri", this species was censused in the ZPS ITA010029 Monte Cofano, Capo San Vito and Monte Sparagio (Trapani province, Sicily) with playback technique between March and April 2011. Superimposing a UTM grid of 1 km mesh on the study area produced cells of 100 hectares. Using a GPS satellite receiver we reached, where possible, the centre of each cell from where the cospecific call was broadcasted. A total of 163 listening stations were implemented. Using software GIS ARCMAP 10.0 (ESRI) presence data were interpolated with vegetational and phytosociological maps (CORINE) to establ…

Sicilian rock partridgeAlectoris graeca whitakeriCensuAnimal Science and ZoologySicilyEcology Evolution Behavior and Systematics
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Note sulle arti decorative a Malta. Inediti argenti siciliani di inizio XIX secolo.

2015

L’articolo si occupa di preziosi e inediti argenti siciliani di inizio Ottocento (ante 1826/1829), tra Rococò e Neoclassicismo, che si trovano a Malta. La maggior parte di essi recano il marchio consolare della città di Catania e sono stati realizzati negli anni 1810-1812. The article deals with precious and unpublished Sicilian silverware of the early nineteenth century (ante 1826/1829), between Rococo and Neoclassicism, that are located in Malta. Most of them bear the consular city mark of Catania and were made in the years 1810-1812.

Silverware decorative arts rococo neoclassicism Sicily MaltaSettore L-ART/02 - Storia Dell'Arte ModernaArgenti arti decorative rococò neoclassicismo Sicilia Malta
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Modelling of segment structures: Boudins, bone-boudins, mullions and related single- and multiphase deformation features

2009

Finite element modelling has been used to simulate the development of segment structures, deformed layer segments separated by veins, such as boudins, mullions, and bone-boudins. A parameter sensitivity analysis is used to compare the influence of the nature of the flow, the relative viscosities of veins in necks and the host rock, and the initial geometry of the layer segments. Parameter fields have been determined for the relative viscosity of veins and layers, and the kinematic vorticity number of flow. Reworked segment structures can have several shapes such as bone-, bulging, shortened bone-boudins and their asymmetric equivalents such as domino- and shearband-boudin geometry. The mode…

Simple shearDeformation (mechanics)GreenschistTension (geology)GeologyGeometryGeotechnical engineeringMullionVorticityShear flowGeologyWall rockJournal of Structural Geology
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